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Table of Contents
Outline
Diagram
Outline
T= Monitoring Faults
1. Devices that Monitor Faults
geologists invented instruments to observe faults that
measure stress/ deformation in crust
**
* creep meter
measures horizontal movement of the ground
laser-ranging device
uses laser beam to detect tiny fault movement
tiltmeter
*
** measures tilting of ground
Satellite Monitor
uses satellite with radar to make images of faults
1. Monitoring Risk in the United States
geologists can't predict when/ where earthquake will strike
usually stress along fault increases until earthquake occurs
sometimes earthquake doesn't occur
earthquake may relieve stress along a another part of a fault
geologists know
earthquakes are likely wherever plate movement stores energy in the rock along faults
geologist can determine earthquake risk
where faults are active
where past earthquakes have occurred
In the United States
risk is highest along Pacific coast
California, Washington, Alaska
Diagram
A diagram of how a laser ranging device works
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Table of Contents
Outline
T= Monitoring Faults
1. Devices that Monitor Faults
- geologists invented instruments to observe faults that
- measure stress/ deformation in crust
*** creep meter
- measures horizontal movement of the ground
- laser-ranging device
- uses laser beam to detect tiny fault movement
- tiltmeter
*** measures tilting of ground
- Satellite Monitor
- uses satellite with radar to make images of faults
1. Monitoring Risk in the United StatesDiagram